自然地理學(xué)專(zhuān)業(yè)英語(yǔ)

1、Lecture 1 INTRODUCTION TO EARTHMajor Concept (I) The planets in our solar system, including Earth, began to form out of a rotating disk of gas and dust about 4.6 billion years ago. Related or supporting concepts:The present view of the beginning of the solar system suggests that a cloud of gas and d

2、ust was flattened into a disk by rotation. The density of the matter in the disk was greatest at its center and decreased toward the edges. The sun formed at the center of the disk where the temperature was highest and the planets formed at greater distances away from the center. The compositions of

3、 the planets differ because of a natural sorting of elements in the cloud with distance from the center. The temperature of the early Earth was probably quite high due to: a. the gravitational capture of particles that released heat on impact, b. the increased pressure on the interior of the planet

4、as it continued to grow, and c. the capture of radioactive elements that gave off heat when they decayed. During the first few hundred million years, the internal temperature rose high enough to melt iron and nickel. These heavy metals sank to form the core of the planet and displaced lighter materi

5、al that rose to form chemically differentiated shells. Major Concept (II) Earths oceans originated early in the planets history. There are two proposed sources of the water in the oceans. Related or supporting concepts: The oldest sedimentary rocks found that required water for their formation are 3

6、.9 billion years old. This suggests that there are been oceans on Earth for roughly 4 billion years.Traditionally scientists have believed that the water in the oceans and atmosphere originated in Earths mantle and was brought to the surface by volcanism.Most magmas contain from 1% to 5% dissolved g

7、as by weight, most of which is water vapor.If we assume that the current rate of release of water vapor in volcanic eruptions has remained essentially constant for the past 4 billion years, then the volume of water expelled(put out) during that time would be roughly 100 times the volume of todays oc

8、eans.A relatively new proposal is that a significant amount of water is added to Earth from space when small icy comets（彗星） enter Earths atmosphere.The early atmosphere did not have any oxygen. The oxygen released from the interior of the planet would have combined with metals at the surface to prod

9、uce oxides.It wasn't until large amounts of oxygen were produced after plants formed that it began to accumulate in the atmosphere.Major Concept (III) There is compelling evidence that there may be other oceans in the solar system. Related or supporting concepts: Two of Jupiters moons, Europa an

10、d Callisto, may have oceans beneath their icy surfaces.Liquid oceans on Europa may be possible despite extremely low temperatures because of heat generated by friction as it is deformed by Jupiters tide-producing gravitational force.Both moons have induced magnetic fields indicating they consist par

11、tly of strongly conducting material. This may be liquid water with electrolytic salts.There is also some indication that Mars once had an ocean covering portions of its northern hemisphere. Major Concept (IV) There are a variety of lines of indirect evidence that allow us to estimate Earths age as b

12、eing about 4.5 to 4.6 billion years. Related or supporting concepts:Earths original crust, that would have formed early in its history, has been destroyed or covered by active volcanism and tectonic processes. This is a reflection of the geologically active nature of the planet. Consequently, the ol

13、dest surface rocks we have found, roughly 4 billion years old, give us a minimum age for Earth rather than an actual age.Indirect evidence of Earths age includes: a. the dating of moon rocks at 4.2 billion years, b. the dating of meteorites at 4.5 to 4.6 billion years, and c. theoretical calculation

14、s of the age of the sun as being roughly the same as the meteorites.We can determine the age of rocks that contain radioactive isotopes of elements that decay at constant, known rates. This is called radiometric dating.If a rock contains atoms of a specific radioactive isotope, half of them will dec

15、ay into another element, called the daughter product, in a period of time called the half-life of the isotope.An example of this type of process would be Uranium235 and its daughter product Lead207 with a half-life of 704 million years. A rock that initially contained 100 atoms of U235 and no Pb207

16、would have the following numbers of the two elements after the indicated elapsed times:There are several different "parent-daughter" radioactive pairs that occur in rocks. Each of the pairs has its own specific half-life, some quite long and others very short. Pairs with long half-lives ar

17、e best for dating very old rocks while those with short half-lives are best for younger rocks. Ideally, an assigned date for a rock will be based on the use of more than one radioactive pair so that a check can be made on accuracy. Major Concept (V) Geologic time is often difficult to grasp because

18、of how long it is compared to all of human history (to say nothing of the incredibly brief time span of a single human life). Related or supporting concepts Just as we divide time into segments like years, months, and days to identify both duration and some sense of position, we divide geologic time

19、 as well. The longest division is called an eon. Eons are divided into eras, eras are divided into periods, and periods into epochs. The geologic time scale and the history of evolution of life-forms is given in table 2.1. The eras, in order of most distant past to most recent time, are: a. Precambr

20、ian, b. Paleozoic (ancient life), c. Mesozoic (intermediate life), and d. Cenozoic (recent life). The divisions of geologic time were originally decided upon on the basis of the appearance and disappearance of specific fossils. The development of radiometric dating techniques allowed geologists to a

21、ssign absolute dates to the different time divisions. Because of the difficulty we typically have in comprehending time spans as great as billions of years, it is often easier to imagine that the earth is much younger, say tens of years old, and then consider what major events occurred in that perio

22、d of time. Suppose, for example, that rather than the earth being 4.6 billion years old, it is only 46 years old. Then we can recognize the following important events:a. 0 years of age: the earth formedb. the first several years of the planet's history have not been preserved in the recordc. 6 y

23、ears of age: the oldest discovered rocks were formedd. 12 years of age: the first living cells appearede. 2223 years of age: photosynthesis began producing oxygenf. 31 years of age: there was sufficient oxygen in the atmosphere to allow the growth of complex cells that require oxygeng. 40 years of a

24、ge: the first hard-shelled organisms appeared, to be preserved later as fossilsh. 41 years of age: the first animals with backbones, called vertebrates, appearedi. 41 years and 8½ months: land plants appeared and were shortly followed by a period of time when fish were the dominant animal formj

25、. 43 years of age: the appearance of reptilesk. 44 years of age: dinosaurs were abundantl. 45 years of age: the dinosaurs disappearedm. about a year ago: flowers appearedn. 4 months ago: mammals, birds, and insects were the dominant life formso. 25 days ago: human ancestors appearedp. 11 days ago: t

26、he first member of the genus Homo appearedq. 30 minutes ago: modern civilization beganr. 1 minute ago: the industrial revolution beganMajor concept (VI) Earth has a roughly spherical shape, bulging slightly at the equator, with a surface that is remarkably smooth. Related or supporting concepts The

27、earth is not a perfectly rigid body. As a result, its rotation causes it to bulge outward at the equator and be slightly flattened at the poles . Approximate values for the following figures are: a. average radius = 6371 km or 3956 mi b. equatorial radius = 6378.4 km or 3961 mi c. polar radius = 635

28、6.9 km or 3947 mi d. (equatorial-polar) radius = 21.5 km or 15 miThe unequal distribution of continents and ocean basins results in a further deformation of the planet from a perfect sphere to a shape that is similar to a pear. Although it seems as if the difference in elevation from the highest poi

29、nt on land to the deepest place on the sea floor is very large, it is really quite small compared to Earths size. The difference in surface elevation is less than 20 km compared to Earth's radius of over 6000 km. If Earth was reduced to the size of a basketball or a grapefruit, its surface would

30、 be about as smooth as they are.Major Concept (VII) Exact position on Earth is determined by latitude and longitude. Related or supporting concepts: A grid of lines can be placed over Earths surface to serve as a reference system to determine location. There are two sets of lines that intersect one

31、another to define latitude and longitude.Lines of latitude are drawn as circles parallel to the equator. These circles have steadily decreasing diameters as they get closer to the poles. Lines of latitude are also called parallels because all of the circles are in planes that are parallel to one ano

32、ther.Latitude is 0° at the equator and increases to 90° at the poles. From this it should be clear that latitude is measured as an internal angle from the center of the Earth away from the equator.By convention, latitudes south of the equator are negative and north of the equator are posit

33、ive.One degree of latitude is equal to 60 nautical miles. Lines of longitude are sometimes called "great circles" because they are drawn by constructing circles perpendicular to the equator, that pass through both poles . In this way, each circle has a diameter that is the same as Earths d

34、iameter. Lines of longitude segment the planet in a way that is similar to the sections of an orange. Lines of longitude are also called meridians. The distance between meridians corresponds to an angle from the center of the earth between an arbitrarily chosen "prime meridian," which is a

35、t 0° by definition, and a second meridian measured along the equator.The prime meridian passes through both poles and Greenwich, England . Longitude can be measured from 0°360° moving eastward from the prime meridian, or from 0° to +180°E and 0° to -180°W. The actu

36、al distance between meridians decreases away from the equator and becomes zero at the poles, where all meridians converge. Each degree of latitude or longitude can be divided into 60 minutes (60) and each minute into 60 seconds (60). Major Concept (VIII) Differences in longitude can be related to di

37、fferences in time between two locations because of Earths rotation. The rotation and revolution of the Earth around the SunRelated or supporting concepts:Earth rotates on its axis once every 24 hours. It follows therefore that it rotates through 360° of longitude each 24 hours. This is equivale

38、nt to (15° of longitude/1 hour) or (15 of longitude/1 minute of time).The time at 0° longitude, or at Greenwich, England is called Greenwich Mean Time (GMT). It is also known as Universal Time (UT) or ZULU (Z) time.The international date line is on the opposite side of the earth from Green

39、wich, England or the prime meridian. It corresponds to the 180° meridian.Because we know the rate of Earths rotation, we can determine our longitude simply by knowing the difference in time between our location and Greenwich, England. For example:Major Concept (IX) Characteristics of Earth'

40、s surface are often shown on maps and charts. 中國(guó)地形圖1：32000000Related or supporting concepts: Maps and charts illustrate three-dimensional shapes on two-dimensional surfaces. Surface features on land are often illustrated with maps. Seafloor features are often illustrated with charts. Charts are also

41、 used to illustrate features in the sky.Three-dimensional features can never be perfectly illustrated on two-dimensional maps and charts. As a result, there is always some distortion of real features. Different map projections will produce different types and degrees of distortion. When choosing a s

42、pecific projection you need to carefully consider which one will produce the least distortion of the features you are interested in. There are three basic types of projections : a. cylindrical, b. conic, and c. tangent plane.The sea floor is often illustrated using a bathymetric chart . Contour line

43、s on a bathymetric chart connect points of equal depth. A chart that shows regions of varying depth by variations in color, shading, or perspective drawing is called a physiographic map. Three-dimensional, color images are generated by computer from detailed sonar data Major Concept (X) Physical, bi

44、ological, and chemical processes on the planet are all influenced by temporal changes or cycles that occur with different periods and are due to Earth's rotation on its axis and its movement around the sun. Related or supporting concepts:There are two natural periods that influence processes on

45、Earth. These are caused by the daily rotation of the planet on its axis which gives us night and day, and the yearly rotation of the earth around the sun which gives us the changing seasons.We experience seasonal variations in climate because Earths rotational axis is tilted away from a line drawn p

46、erpendicular to the plane of its orbit around the sun by 23½°. Earths tilt results in an annual migration of the apparent position of the sun in the sky from being directly overhead at noon somewhere between 23½°S and 23½°N throughout the year. Outside of this band of l

47、atitude centered on the equator, the sun will never appear to be directly overhead even when it has risen in the sky to its highest point at noon.The Northern Hemisphere is tilted toward the sun during Northern Hemisphere summers and is warmer because the intensity of solar radiation is greater at t

48、he surface when the sun's rays are more nearly perpendicular to the surface. At this time the Southern Hemisphere experiences its winter as it is tilted away from the sun. There are four parallels of latitude that have special names; these are: Latitude Name 66½°N Arctic Circle 23½

49、;°N Tropic of Cancer 23½°S Tropic of Capricorn 66½°S Antarctic Circle On the summer solstice, which usually occurs around June 22, the sun will be directly overhead the Tropic of Cancer and there will be 24 hours of daylight above the Arctic Circle. This is the day with the

50、longest period of daylight in the Northern Hemisphere and the shortest in the Southern Hemisphere. The sun will not rise at all at latitudes farther south than the Antarctic Circle. On the autumnal equinox, on about September 23, the sun will be directly overhead the equator and the amount of daylig

51、ht will be the same everywhere.On the winter solstice, around December 21, the sun will be directly overhead the Tropic of Capricorn and there will be 24 hours of daylight above the Antarctic Circle and perpetual darkness above the Arctic Circle. This will be the day with the longest period of sunli

52、ght in the Southern Hemisphere and the shortest in the Northern Hemisphere. On the vernal equinox, roughly March 21, the sun will have moved northward again to stand directly over the equator. The greatest annual change in climate occurs at mid-latitudes in what are called the temperate zones. At lo

53、w latitudes it is relatively warm throughout the year and at high latitudes it remains fairly cold. The orbit the earth takes around the sun is elliptical, so the distance between the earth and the sun changes through the year. The distance is greatest during the Northern Hemisphere summer and least

54、 during the Northern Hemisphere winter. It is important to remember that the seasons are not due to the variable distance from the sun (otherwise we should expect summer in the Northern Hemisphere when we are closest to the sun in the end of December), but rather they are controlled by what hemisphe

55、re is tilted toward the sun's rays.Major Concept (XI) Earth is essentially a closed system. As such, all of the water available to the planet moves through different reservoirs where it is stored for varying periods of time before moving on. Related or supporting concepts:Water can be found in a

56、ll three states of matter in the earth system: solid (ice), liquid, and gas (water vapor). At any given time a water molecule will be located in a specific reservoir. Examples of reservoirs include the atmosphere, rivers, lakes, the oceans, glaciers, and groundwater, to name a few. Water will not re

57、main indefinitely in a single reservoir; rather, it will be cycled from one reservoir to another by such processes as evaporation, precipitation, transpiration, sublimation, and runoff. Transpiration is the release of water by plants. Sublimation is a phase change of water from solid to gas, or from ice to water vapor. The cycling of water from one reservoir to another is called the hydrologic cycle. The hydrologic cycle can be seen di